A&A 468, L25-L28 (2007)
DOI: 10.1051/0004-6361:20077294
Letter
The water ice rich surface of (145453) 2005 RR
:
a case for a
carbon-depleted population of TNOs?
N. Pinilla-Alonso1, J. Licandro2, 3, R. Gil-Hutton4, and R. Brunetto5, 6 1 Fundación Galileo Galilei & Telescopio Nazionale Galileo, PO Box 565, 38700, S/C de La Palma, Tenerife, Spain
e-mail: npinilla@tng.iac.es
2 Isaac Newton Group, 38700 Santa Cruz de La Palma, Tenerife, Spain
3 Instituto de Astrofísica de Canarias, c/Vía Láctea s/n, 38205 La Laguna, Tenerife, Spain
4 Complejo Astronómico El Leoncito (Casleo) and San Juan National University, Av. España 1512 sur, J5402DSP, San Juan, Argentina
5 Dipartimento di Fisica, Università del Salento, via Arnesano, 73100 Lecce, Italy
6 INAF-Osservatorio Astrofisico di Catania, via S. Sofia 78, 95123 Catania, Italy
(Received 13 February 2007 / Accepted 23 April 2007)
Abstract
Context.Recent results suggest that there is a group of trans-Neptunian objects
(TNOs) (2003 EL61 being the biggest member), with surfaces composed
of almost pure water ice and with very similar orbital elements. These
objects provide exciting laboratories for the study of the processes that
prevent the formation of an evolved mantle of organics on the surfaces of
the bodies in the trans-Neptunian belt (TNb).
Aims.We study the surface composition of another TNO that moves in a similar
orbit, (145453) 2005 RR43, and compare it with the surface composition
of the other members of the group.
Methods.We report visible and near-infrared spectra in the 0.53-2.4
m
spectral range, obtained with the 4.2 m William Herschel Telescope and
the 3.58 m Telescopio Nazionale Galileo at the "Roque de los Muchachos"
Observatory (La Palma, Spain). Scattering models are used to derive
information about its surface composition. We also measure the depth D
of the water ice absorption bands and compare with those of the other
members of the group.
Results.The spectrum of 2005 RR43 is neutral in color in the visible and
dominated by very deep water ice absorption bands in the near infrared
(
% and
at 1.5
m and 2.0
m
respectively). It is very similar to the spectrum of the group of TNOs
already mentioned. All of them present much deeper water ice absorption
bands (
) than any other TNO except Charon. Scattering models show
that its surface is covered by water ice, a significant fraction in
crystalline state with no trace (5% upper limit) of complex organics.
Possible scenarios to explain the existence of this population of TNOs
are discussed: a giant collision, an originally carbon depleted composition,
or a common process of continuous resurfacing.
Conclusions.2005 RR43 is member of a group, may be a population, of TNOs
clustered in the space of orbital parameters that show abundant water ice
and no signs of complex organics and which origin needs to be further
investigated. The lack of complex organics in their surfaces suggests
a significant smaller fraction of carbonaceous volatiles like CH4
in this population than in "normal" TNOs. A carbon depleted population of TNOs could be the origin of
the population of carbon depleted Jupiter family comets already noticed by A'Hearn et al. (1995).
Key words: Kuiper Belt -- solar system: formation
© ESO 2007

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